Fourier Theory in Seismic Processing

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Fourier Theory in Seismic Processing (From Liner and Ikelle and Amundsen) • Temporal aliasing • Spatial aliasing

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Fourier Theory in Seismic Processing. (From Liner and Ikelle and Amundsen). Temporal aliasing Spatial aliasing. Sample Rates. What is the fewest number of times I need to sample this waveform per second?. ?. ?. ?. Sample Rates. Sample Rates. Sample Rates. Sample Rates. - PowerPoint PPT Presentation

Transcript of Fourier Theory in Seismic Processing

Page 1: Fourier Theory in Seismic Processing

Fourier Theory in Seismic Processing

(From Liner and Ikelle and Amundsen)

• Temporal aliasing• Spatial aliasing

Page 2: Fourier Theory in Seismic Processing

Sample Rates

What is the fewest number of times I need to sample this waveform per second?

?

?

?

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Sample Rates

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Sample Rates

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Sample Rates

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Sample Rates

What is the fewest number of times I need to sample this waveform per second?

At least twice per wavelength or period!

OTHERWISE ….

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Undersampled waveforms

True frequency (f -true)

Am

plit

ud

e

Reconstructed frequency

(f -aliased)

ff

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Oversampled waveforms

= True frequency (f -true)

Am

plit

ud

e

Reconstructed frequency

frequency is unaliased

Nyquist frequency

Nyquist frequency = 1 / twice the sampling rate

Minimum sampling rate must be at least twice the desired frequency

E.g., 1000 samples per second for 500Hz,

2000 samples per second for 1000 Hz

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Oversampled waveformsA

mp

litu

de Nyquist frequency

In practice we are best oversampling by double the required minimum

i.e. 1000 samples per second for a maximum of 500 Hz

i.e., 2000 samples per second for a maximum of 1000 Hz

Oversampling is relatively cheap.

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Spatial frequency, or wavenumber (k) is the number of cycles per unit distance.

One spatial cycle or wavenumber = frequency/velocity.

Each wavenumber must be sampled at least twice per wavelength

(two CMP’s per wavelength)

Spatial aliasing

1

2( )kN CMPspacing

IN PRACTICE each wavenumber must be sampled at least four times per minimum

wavelength (two CMP’s per wavelength)

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Spatial aliasing

However, dip (theta) as well as frequency and velocity event changes the number of cycles per distance, so

4sin

lambdaCMPinterval

Liner, 9.7,p.192

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Spatial aliasing

4sin

lambdaCMPinterval

x

V t

limitsinV t

x

For aliasing NOT to occur, delta(t) must be less than T/2

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Spatial aliasing

limitsin2

VT

x

lim 2sinit

VTx

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Geophone Spacing and Spatial Aliasing

K=0

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1/4 wavelength shift per trace

total shift across array=3/4 wavelength

K=+ or -ve?

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1/4 wavelength shift per trace

total shift across array=3/4 wavelength

K=?

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1/2 wavelength shift per trace

total shift across array=3/2 wavelength

K=0

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3/4 wavelength shift per trace

total shift across array=2 1/4 wavelength